Dictionary:Airy-Heiskanen isostasy

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{{#category_index:A|Airy-Heiskanen isostasy}} (er’ ē hī skan’ ∂n ī sos’ t∂ sē). A modification of the Airy isostatic hypothesis. Usually assumes that compensation is complete and local, that the Earth’s crustal density is 2.67 g/cm3, and that the density of the layer under the crust is 0.6 g/cm3 higher than that of the crust. See isostasy and Figure I-7.